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  Boron speciation in aqueous fluids at 22 to 600°C and 0.1 MPa to 2 GPa

Schmidt, C., Thomas, R., Heinrich, W. (2005): Boron speciation in aqueous fluids at 22 to 600°C and 0.1 MPa to 2 GPa. - Geochimica et Cosmochimica Acta, 69, 2, 275-281.
https://doi.org/10.1016/j.gca.2004.06.018

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Item Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_231604 Version Permalink: -
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Schmidt, Christian1, Author              
Thomas, Rainer1, Author              
Heinrich, Wilhelm1, Author              
4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, Author              
4.2 Inorganic and Isotope Geochemistry, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, Author              
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13.3 Chemistry and Physics of Earth Materials, 3.0 Geodynamics and Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146036              

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 DDC: 550 - Earth sciences
 Abstract: <P>The speciation of boron in H<FONT SIZE="-1">2</FONT>O+H<FONT SIZE="-1">3</FONT>BO<FONT SIZE="-1">3</FONT>±NaCl and H<FONT SIZE="-1">2</FONT>O+Na<FONT SIZE="-1">2</FONT>B<FONT SIZE="-1">4</FONT>O<FONT SIZE="-1">7</FONT> fluids was studied in situ at temperatures between 22 and 600°C and pressures from 0.1 MPa to about 2 GPa using Raman spectroscopy and a hydrothermal diamond anvil cell. Additionally, we determined the frequency shifts of the 877 cm-1 Raman line of [B(OH)<FONT SIZE="-1">3</FONT>]0 in aqueous fluids with temperature (<FONT FACE="Math1">d</FONT><FONT FACE="Math5">v</FONT><FONT SIZE="-1">877</FONT>/<FONT FACE="Math1">dT</FONT>)<FONT SIZE="-1">P=0.1 MPa</FONT> = -0.02532 cm-1K-1 and pressure (<FONT FACE="Math1">d</FONT><FONT FACE="Math5">v</FONT><FONT SIZE="-1">877</FONT>/<FONT FACE="Math1">d</FONT>P)<FONT SIZE="-1">T=22°C</FONT> = 4.06 cm-1GPa-1. The observed species in acidic fluids were [B(OH)<FONT SIZE="-1">3</FONT>]0 and smaller amounts of a four-coordinated boron species which may be attributed to dissolved metaboric acid HBO<FONT SIZE="-1">2</FONT>(aq). The ratio of this B[4]-O species to [B(OH)<FONT SIZE="-1">3</FONT>]0 increases with temperature and decreases slightly with addition of NaCl. In alkaline solutions, polyboric ions depolymerize rapidly with temperature. Thus, [B(OH)<FONT SIZE="-1">3</FONT>]0 and [B(OH)<FONT SIZE="-1">4</FONT>]- were the only remaining detectable species at 500 and 600°C. The Raman spectra showed an increase of [B(OH)<FONT SIZE="-1">3</FONT>]0 relative to [B(OH)<FONT SIZE="-1">4</FONT>]- with temperature and an increase of [B(OH)<FONT SIZE="-1">4</FONT>]- relative to [B(OH)<FONT SIZE="-1">3</FONT>]0 with pressure. <BR> The general trend in the boron speciation is a higher stability of simpler complexes with temperature. The experimental observations strongly indicate that planar three-coordinated [B(OH)<FONT SIZE="-1">3</FONT>]0 is the predominant boron species in the aqueous phase over a wide range of P-T-pH conditions. This supports the validity of previous assumptions on boron coordination in crustal and mantle wedge fluids.<BR> </P>

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 Dates: 2005
 Publication Status: Finally published
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 Identifiers: eDoc: 5938
GFZPOF: 2.0 Geodynamik, Stoffkreisläufe und Ressourcen
DOI: 10.1016/j.gca.2004.06.018
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Title: Geochimica et Cosmochimica Acta
Source Genre: Journal, SCI, Scopus
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Pages: - Volume / Issue: 69 (2) Sequence Number: - Start / End Page: 275 - 281 Identifier: CoNE: https://gfzpublic.gfz-potsdam.de/cone/journals/resource/journals161